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| Artículos de revistas
Soil carbon balance in a tropical grassland: Estimation of soil respiration and its partitioning using a semi-empirical model
dc.creator | Caquet, B. | |
dc.creator | De Grandcourt, A. | |
dc.creator | M'bou, A. Thongo | |
dc.creator | Epron, D. | |
dc.creator | Kinana, A. | |
dc.creator | Saint Andre, L. | |
dc.creator | Nouvellon, Y. | |
dc.date.accessioned | 2013-11-05T11:45:49Z | |
dc.date.accessioned | 2018-07-04T16:20:49Z | |
dc.date.available | 2013-11-05T11:45:49Z | |
dc.date.available | 2018-07-04T16:20:49Z | |
dc.date.created | 2013-11-05T11:45:49Z | |
dc.date.issued | 2012 | |
dc.identifier | AGRICULTURAL AND FOREST METEOROLOGY, AMSTERDAM, v. 158, n. 6, supl. 1, Part 1, pp. 71-79, 42156, 2012 | |
dc.identifier | 0168-1923 | |
dc.identifier | http://www.producao.usp.br/handle/BDPI/41254 | |
dc.identifier | 10.1016/j.agrformet.2012.02.008 | |
dc.identifier | http://dx.doi.org/10.1016/j.agrformet.2012.02.008 | |
dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/1634661 | |
dc.description.abstract | In savannah and tropical grasslands, which account for 60% of grasslands worldwide, a large share of ecosystem carbon is located below ground due to high root:shoot ratios. Temporal variations in soil CO2 efflux (R-S) were investigated in a grassland of coastal Congo over two years. The objectives were (1) to identify the main factors controlling seasonal variations in R-S and (2) to develop a semi-empirical model describing R-S and including a heterotrophic component (R-H) and an autotrophic component (R-A). Plant above-ground activity was found to exert strong control over soil respiration since 71% of seasonal R-S variability was explained by the quantity of photosynthetically active radiation absorbed (APAR) by the grass canopy. We tested an additive model including a parameter enabling R-S partitioning into R-A and R-H. Assumptions underlying this model were that R-A mainly depended on the amount of photosynthates allocated below ground and that microbial and root activity was mostly controlled by soil temperature and soil moisture. The model provided a reasonably good prediction of seasonal variations in R-S (R-2 = 0.85) which varied between 5.4 mu mol m(-2) s(-1) in the wet season and 0.9 mu mol m(-2) s(-1) at the end of the dry season. The model was subsequently used to obtain annual estimates of R-S, R-A and R-H. In accordance with results reported for other tropical grasslands, we estimated that R-H accounted for 44% of R-S, which represented a flux similar to the amount of carbon brought annually to the soil from below-ground litter production. Overall, this study opens up prospects for simulating the carbon budget of tropical grasslands on a large scale using remotely sensed data. (C) 2012 Elsevier B.V. All rights reserved. | |
dc.language | eng | |
dc.publisher | ELSEVIER SCIENCE BV | |
dc.publisher | AMSTERDAM | |
dc.relation | AGRICULTURAL AND FOREST METEOROLOGY | |
dc.rights | Copyright ELSEVIER SCIENCE BV | |
dc.rights | closedAccess | |
dc.subject | TROPICAL GRASSLAND | |
dc.subject | SOIL RESPIRATION | |
dc.subject | LAI | |
dc.subject | APAR | |
dc.subject | PARTITIONING | |
dc.subject | SEASONAL VARIATION | |
dc.title | Soil carbon balance in a tropical grassland: Estimation of soil respiration and its partitioning using a semi-empirical model | |
dc.type | Artículos de revistas |